Overturning the circulation of the ocean - Dr. Ali Mashayek (MIT)

Date & time

2–3pm 28 March 2017


Hales Room, J7


Dr. Ali Mashayek (MIT)


 Kial Stewart

It has been an open question whether turbulent vertical mixing across density surfaces is sufficiently large to play a dominant role in closing the deep branch of the ocean meridional overturning circulation. This talk will consist of four parts: (I) By means of a cascade of observationally-tuned nested high resolution realistic numerical simulations of turbulent mixing of tracers in the Southern Ocean I will show that the fast vertical spreading of tracers occurs when they come in contact with mixing hotspots over rough topography. The sparsity of such hotspots is made up for by enhanced tracer residence time in their vicinity due to diffusion toward weak bottom flows; (II) I will further argue that the net vertical mixing in energetic turbulent zones is likely the residual of interior sinking (contrary to the commonly assumed interior upwelling induced by breaking internal waves) and larger boundary upwelling; (III) I will show that the potential implication of these findings is to reshape our understanding of abyssal circulation in a way that may explain the large vertical fluxes of heat and salt required to close the global abyssal circulation; (IV) I will finish by discussing some ongoing work focused on exploring climatic implications of the aforementioned findings.

Updated:  26 May 2018/Responsible Officer:  RSES Webmaster/Page Contact:  RSES Webmaster